Next Article in Journal
Towards a Healthy Car: UVC LEDs in an Automobile’s HVAC Demonstrates Effective Disinfection of Cabin Air
Previous Article in Journal
Analysis of the Spatial–Temporal Distribution Characteristics of NO2 and Their Influencing Factors in the Yangtze River Delta Based on Sentinel-5P Satellite Data
 
 
Font Type:
Arial Georgia Verdana
Font Size:
Aa Aa Aa
Line Spacing:
Column Width:
Background:
Communication

Thoughts about the Thermal Environment and the Development of Human Civilisation

by
Ioannis Charalampopoulos
1,* and
Andreas Matzarakis
2,3
1
Laboratory of General and Agricultural Meteorology, Agricultural University of Athens, Iera Odos 75, 11855 Athens, Greece
2
Research Centre Human Biometeorology, German Meteorological Service, D-79104 Freiburg, Germany
3
Department of Earth and Environmental Sciences, Faculty of Environment and Natural Resources, University of Freiburg, Werthmannstr. 10, D-79085 Freiburg, Germany
*
Author to whom correspondence should be addressed.
Atmosphere 2022, 13(11), 1925; https://doi.org/10.3390/atmos13111925
Submission received: 24 October 2022 / Revised: 14 November 2022 / Accepted: 15 November 2022 / Published: 18 November 2022
(This article belongs to the Section Biometeorology and Bioclimatology)

Abstract

:
Thermal conditions are the most challenging factors in studying human biometeorology, indoor and outdoor design, and adaptation to climate change. The thermal environment is always present and shapes everyday life, behaviours, and the natural and artificial environment. In this paper, we analyse some thoughts that link thermal perception to the roots of human civilisation. Following the narrative thread of mythology and the history of religions, there are direct and indirect references to the thermal environment everywhere. The thermal environment may be a part of the core of human culture.

1. A Short Introduction about the Impact of Climate and Weather on Human Life

The atmospheric environment has been of concern to human life since the beginning of civilisation. This is because it is a part of the environment that affects civilisation directly, indirectly, and constantly since it exists wherever humankind exists [1,2]. From primitive human creations to the most complex expressions of art, the atmospheric environment seems to play a significant role. Before humans developed the sciences, they interpreted the elements and phenomena of the atmosphere as an expression of desire, the disposition of the gods, or other supernatural forces [3,4]. The thunderbolt was the symbol of Zeus; with it, he punished. Neptune created storms when he was angry. The clouds opened for God’s angel to appear or for the voice of God to be heard. The flood comes to destroy the old world, and, in its place, a new one is created. The dust devil is some deity who looks like the lamp genie and can achieve supernatural things. The atmosphere and its various phenomena appear very often in poetry, literature, and music [5,6,7,8]. It is also one of the main factors that determined the way in which houses were built and the layout of cities [9,10,11,12,13].
If we look more systematically at the effects of atmospheric conditions on human civilisation’s development, we can see that they are present everywhere. Obviously, the local climate has considerably influenced the location and development of organised settlements (villages to cities) [14,15,16]. Moreover, Hippocrates recommended that weather and climate be considered in developing settlements [17]. In essence, we have the appearance of the first settlements where the climate was favourable at the time when humankind left nomadic life to become farmers and herdsmen. The atmospheric environment was one of the primary shapers of the possible choices for a group of people to settle in a specific place. It affected the availability of critical resources such as water and food, as well as the residents’ safety. As humans developed their technical/technological civilisation, they could protect or even utilise the atmospheric environment to benefit their better living. Humans’ technical means and developments have allowed for the expansion of possible dwelling places and accommodations in less hospitable climatic environments. The climate and its changes may have affected even the organisation’s parts and subsystems. Climate has influenced many aspects of human civilisation; humans not only observe (now measure and record) weather and climate but also feel them. In fact, humankind’s unconscious and most conscious decisions are not linked to their knowledge of climate and weather but are related to what the human body feels about atmospheric conditions. This is why humans have sensory organs in their body that allow them to perceive the atmospheric situation. This sense of the atmospheric environment and its changes enables the human body to react and adapt to survive while maintaining good functioning [18,19,20,21]. Therefore, the perception and sense of the thermal environment are of primary importance since it affects the core of human existence.
Despite the obvious importance of the thermal environment in the quality of human life, the concept of the sense of hot/cold began to be studied in the late 19th and early 20th centuries [22,23]. Furthermore, after World War II, efforts to analyse human physiology related to the human sense of the thermal environment became more intensive [18,24]. The findings of relevant studies showed that more and more human activities were directly and indirectly affected by the thermal environment and thermal sensation, such as work performance, entertainment, psychology, and human health in general [21,22,23,25,26]. The importance of the thermal environment soon led to the creation of biometeorological indices to quantify thermal conditions and the corresponding response of the human body to them [9,18,27,28]. Over time, these indices became more complex and accurate, while the spread of personal computers (PCs) made it possible to develop complex human energy balance models [19,29,30,31,32]. Today, with the help of the prevailing indices, human biometeorology can be applied in the design of outdoor or indoor spaces and in the assessment of the thermal load on humans during their stay in various configurations and situations [33,34,35,36].
While discoveries and developments in human biometeorology offer more accurate estimates of the interaction of humans with their thermal environment, the scientific debate about how deep the thermal sense lies in the origins of human civilisation has not yet begun. This paper aims to analyse in a narrative how strongly the evolution of human civilisation is linked to the perception of the human thermal sense. Since the factors that are connected to so-called human civilisation are numerous, we selected some of the most prevalent.

2. The Thread of Thermal Perception in Human History and Civilisation

Thermal sensation, thermal perception, thermal stress, and all expressions of the human biometeorological environment are present at every moment of the day [37]. This is the reason why its effect on health, psychology, and even human behaviour is not easily perceived.
More specifically, weather and climate have played a decisive role in many human activities throughout history. A significant number of studies have shown the influence of weather and climate on the evolution of human history. Atmospheric conditions can be traced in art, music, painting, and literature [8,38,39,40,41]. The atmospheric conditions also determined, to a significant extent, the location of settlements, the development of productive activities, and the possibility of trade and communication [36,42,43,44,45,46,47,48]. There are many recorded cases where climate determined the development, evolution, or even the end of a civilisation (Incas, Minoans, etc.) [49,50,51,52,53,54]. Meteorological conditions have even played a decisive role in world history in judging battles or war developments [49,55,56,57,58,59].
Biometeorological conditions, i.e., meteorological conditions on a shorter timescale that have influenced biological organisms in shaping our culture over time, seem to have played a significant role. To understand the influence of biometeorological conditions and thermal sensation on the various areas of human life, it is worth analysing the temporal evolution of the relevant individual influences from the present to the past. It is more accurate to say that human health and behaviour are influenced by the human heat balance and thermal sensation. In general, people need and prefer conditions of 20–23 °C to feel good and have thermal equilibrium. This temperature range ensures good body function and health promotion and ensures high work productivity. The distance from the thermal equilibrium state negatively affects human health in a proportional but not linear relationship. The health burden from thermal stress (either due to cold or warm conditions) increases morbidity and mortality. The magnitude and rate of increase are obviously related to the prevailing biometeorological conditions and to each individual’s characteristics and biological conditions [35,60,61,62,63,64,65,66].
Despite the apparent importance of the human thermal sense and perception, only a few decades ago, the attempt to quantify thermal comfort and human perception of their thermal environment began. According to Gagge et al. [22], since 160 AD, the importance of the sense of hot and cold has been understood. In the same work, the authors stated that “comfort is a recognisable state of feeling, but possesses no identifiable sense organ like the basic five senses”. Today, measurements and human biometeorological models are used in urban planning, outdoor space design, and parks and other recreational areas such as stadiums and sports facilities [27,31,32,60]. Biometeorological observations are also applied to design residential interiors, offices, and workplaces [35,60,67]. The information on thermal comfort/feeling and heat stress is valuable and concerns humans directly and indirectly. The direct effect relates to how people feel and how this impacts their psychology, productivity, and health. Therefore, by creating satisfactory biometeorological conditions in open or closed spaces, the individual’s health, productivity, and psychology are improved [42,48,68,69]. In the era of climate change, the effect of heat, especially heat waves in the human health context and the increase in mortality and morbidity are mainly focused on developing strategies for protecting human health [66,70]. The indirect effect of biometeorological conditions is extremely important to humans and relates to energy consumption to achieve satisfactory thermal comfort conditions. Given that thermal comfort is a human need, large sums are spent on heating and cooling to create satisfactory conditions [71,72,73].
There are frequent reports from studies of the effect of weather on humans in the short and long term. It has been found that weather can affect human health, behaviour, and choices. However, the human body reacts to the thermal environment and adapts to maintain health and functionality. However, the human organism and its reactions differ according to age, gender, health status, and physical condition, which are parameters taken into account in modern biometeorological indicators such as PET, mPET, and UTCI [30,31,32,35,74,75,76,77,78,79,80,81,82]. It is, therefore, simplistic to consider that weather affects human health and behaviour.

2.1. Buildings and Built Environment

Our houses are built with biometeorological principles, whether consciously or empirically. From the beginning, humans sought a place to live to protect themselves from adverse weather conditions and wild animals that threatened them. In essence, they looked for a place that offered containment and protection, as well as more satisfactory atmospheric conditions than those found in the countryside. The first shelters were usually caves and recesses in rocks and were often sheltered near or in trees. They lit a fire at night to temper the cold conditions and to keep unwanted animals away. Later, humans were able to make makeshift shelters from animal skins and furs, which they erected in the areas they hunted and dismantled to take with them to the next hunting ground [83,84,85]. When people abandoned the nomadic life and became farmers and herders, they began to build more complex structures of a permanent character. Obviously, the materials they used were readily available, such as stone, mud, bricks, and wood. The first purpose that the buildings had to perform was protection from the weather and enemies (animals and people). As technology developed, people could use more natural materials, create artificial materials, and transport raw materials over greater distances.
The development of technological civilisation gradually led to the differentiation of the construction of houses built by people from region to region, according to criteria which, among other things, had to do with maintaining thermal comfort inside the houses [86,87]. Keeping indoor conditions at tolerable levels for humans helped maintain a better state of health when medicine was less developed. One with a better dwelling in terms of indoor thermal conditions was likely to have better health. In temperate climates such as the Mediterranean, the main concern during cold periods of the year was to have adequate light, heating, and heat retention. In contrast, during the warmer periods of the year, the concern was protection from the sun and air renewal to maintain cool conditions. For these reasons, these climates had relatively large windows of appropriate orientation and shape, and the buildings were lightweight constructions. In warmer climates, the main focus was on shading during most of the day since exposure to the sun created conditions far from thermal comfort. These buildings often had high walls designed to provide shading and vertical air movement so that warm air would rise high and exit the building and be replaced by cooler air from lower levels. On the contrary, in areas of the world with a cold climate, buildings were built with thick walls (made of stone or other materials) with small and few openings. Often buildings were sunk into the ground or rock to reduce heat loss, and there are cases where earth covered low-rise buildings up to the roof. These structures aimed to keep heat inside and provide the best possible insulation from the outside environment. In all cases, the buildings were built to provide thermal conditions as close to thermal comfort as possible for as long as possible [83,84,86,87,88,89,90,91,92]. That is, the structure and form of the buildings were determined by the need to maintain a satisfactory thermal sense of their inhabitants. It should be noted that long-term acclimatisation of their inhabitants took place along with the adaptation of buildings to local thermal conditions. It would be difficult for a resident of a hot desert to live in a traditional Icelandic house and vice versa.
Thermal perception is very individual, and people sometimes prefer cool or warm conditions according to their state of health, psychology, previous physical activity, gender, acclimatisation, clothing, and medal condition [18,32,64,93,94,95,96,97]. Apart from the indoor built environment, humankind’s thermal perception also influenced the outdoor environment and the layout of their settlements. When the citizens walk in cities under intense sunshine, they follow the route with the most shade. Many modern studies have shown that shading is the key factor in improving the thermal sensation of humans in warm environments with high sunshine duration [90,98,99,100,101]. The need for shading, which determines human thermal comfort, is one of the main factors that shaped traditional architecture and open space configurations, such as that of the Aegean islands in Greece or the regions of North Africa. The main characteristics of these configurations are the narrow streets and high walls surrounding the buildings and the courtyards [102,103,104,105,106].
Conversely, in areas with less sunshine, where the presence of solar radiation is desirable, traditional or even modern urban planning includes a wider street width and a generally shallower urban canyon [107,108,109,110,111]. Modern and mainly traditional human settlements have generally adapted to the needs for a thermal environment as close to optimal as possible. Therefore, both the indoor built environment and the outdoor environment, two essential elements of human culture, have been and still are influenced by humankind’s need for thermal balance.

2.2. Energy Requirements

From the very beginning of their existence, humans sought a way to heat the space they lived in and keep aggressive animals away. The first solution to these two issues was the discovery of fire. This was the beginning of humankind’s systematic energy consumption (other than food). Technological development has led to the rapid demand for energy to feed transportation, industry, production processes, lighting, heating and cooling water, and indoor spaces. However, most of the energy consumed by households today is spent on heating, which is directly linked to thermal sensation [71,112,113,114,115]. In fact, the amounts spent on heating and cooling indoors are directly related to how the inhabitants feel about their thermal environment at any given time. That is, it does not depend on the area’s climate but on what the inhabitants feel at any given time. The distribution of energy resources today shapes the global geopolitical arena, triggers wars, and largely determines nations’ economies. The need for energy leads to new technological discoveries while simultaneously intensifying the phenomenon of climate change (through the release of greenhouse gases) [72,113,116]. Another critical factor of human civilisation, over time, is dependent on humankind’s perception of their thermal environment.

2.3. Clothing

The clothes we wear are determined by the biometeorological conditions, i.e., the thermal sense of the human body. Humans originally created clothes to protect them from atmospheric conditions. From the earliest days of humankind’s appearance as a hunter–gatherer, they moved from place to place and, as a result, had no permanent shelter. As a result, they were constantly exposed to the weather. They removed the skin from the animals they killed to feed themselves and used it as the first garment. This practice allowed humans to protect themselves from inclement weather and survive in areas where they could not otherwise. Clothing is an additional insulating layer that allows humans to explore more areas and exploit more environmental resources found in areas with unfriendly climatic conditions. [83,88,117]. After animal skin and fur, humans discovered or created other materials to make clothes, such as flax, wool, and cotton, which could form thinner layers of effective clothing when processed. The clothing available to humankind protected them not only from cold but also from intense sunlight and high temperatures. As long as humans could have effective clothing to regulate their thermal sense, they could explore and inhabit more areas. This ability led to the colonisation of new areas, resulting in an increase in the world’s population and the development of more civilisations. The need for thermoregulation and protection from extreme co-conditions led to the creation of a means that at first was through survival but later became much more. Today, clothing is one of the basic elements that make up any culture and can also symbolise power, social class, or status [18,118,119,120,121,122]. However, whatever the clothing we wear daily, it is definitely and primarily a means of regulating our thermal sensation. Thus, the need to regulate humankind’s thermal environment initially created and subsequently led to the evolution of a wide variety of clothing that is ultimately an important part of the tradition and culture of people.

2.4. Language

The languages spoken by humans and their sounds are influenced by many non-linguistic factors, which are environmental and topographical [123,124]. It has been found that, in dry and cold environments, people develop and speak languages with fewer vowels as a result of the effect of atmospheric conditions on the vocal cords and larynx. Conversely, in areas of increased humidity and heat, the languages spoken by people have more vowels. Scientists believe that in addition to the effect of thermogravimetric conditions on the physiology and function of the speech organs, it is also important to determine how far the sound can reach and be heard clearly. Therefore, in areas of relatively high temperature and humidity, which are often rich in vegetation, growing languages have more vowels and can be heard more clearly despite the presence of trees or water that absorb sound [123,124,125,126,127,128]. It remains to be examined the possibility that the existence of vowels is linked to humankind’s thermal comfort since they lose heat through breathing and the opening of the mouth [18,129]. Therefore, thermal balance is regulated with the environment. This oral heat loss function can be a critical body heat reduction function for populations living in areas of high temperature and humidity. It should be kept in mind that high humidity reduces the effectiveness of the heat loss process through perspiration.
Conversely, in low-temperature and dry environments, a closed mouth (i.e., few vowels) may reduce heat loss from the mouth area. Lastly, it is possible that, in addition to how far the sound of the voice reaches, it is also possible that the maintenance of the human heat balance is essential. Reducing body heat in warm environments and retaining it in cold ones is vital, especially in the past when humans did not have the insulated buildings and clothing available to them today. Hence, we can assume a possible connection between the thermal environment and the language sound, especially under extreme climatic conditions, since respiration is one of the most prominent thermoregulation functions. Humans may have altered their language sounds in their effort to maintain their thermal equilibrium with their environment. Thus, thermal perception can influence the language spoken by a people, which is a critical element of their culture.

2.5. From Social Life to Philosophy

Social life in the early stages of the development of civilisation was directly dependent on the thermal environment. The place where small or large groups of people met, exchanged opinions, and made decisions was the marketplace of each city, called Agora. This was basically an open-air place where trade took place while, at the same time, citizens met and learned about news and problems. How often they could do this depended on the weather. How long they could stay in this marketplace depended on how comfortable they felt in this outdoor space. Later, when the system of government of democracy was devised, it was necessary for citizens to meet, consult on the issues of their concern, and finally vote to make decisions. For this to happen, all the citizens who had the right to vote had to gather in one place for several hours. Historically, the place where democracy emerged and developed in ancient Athens and the place of deliberation was the rock of the Pnyx next to the Acropolis (Figure 1). Athens, then as now, had good weather for much of the year, allowing citizens to stay outdoors. It seems that the biometeorological environment played a role in discovering democracy and its early operational stages.
Therefore, the possibility of gathering citizens and their communication, i.e., the exchange of views and recreation, was linked in those years to the time they could be in the marketplace and chat. In addition to the apparent relationship that the system of government of the ancient Greek democracy, which was based on the possibility of all citizens voting for decision making, we find another decisive relationship between the bioclimate and the development of civilisation, which is the ancient philosophical schools. These were where all citizens who were interested in and conversed about matters relating to life and philosophy gathered. This was under the supervision and teaching of a philosophical teacher. Most of these schools were nothing more than groups of people gathering in open spaces, often under trees, to protect themselves from the Greek sun and think and discuss philosophy [130,131].
Plato’s famous academy was a garden where all the students gathered, and, in this beautiful and comfortable environment, they developed their philosophical thoughts [132]. Moreover, Aristotle’s philosophy school was called Peripatetic (walking) because the master and the students walked in the open space (gardens, market etc.) and discussed their preferred topics [133,134,135]. The prerequisite for these important schools of thought to function was the concentration of people in a pleasant environment of comfort. Furthermore, this comfort was predominantly thermal comfort and, in some cases, aesthetic comfort.

2.6. Mythology and Religions

Human civilisation is interwoven with great and important narratives. These came from mythology and religion. Both include, among other things, rules of life and teachings that help society function better. The mythology and sacred texts of religions include moral rules and lead to thoughts on how humans should function and coexist. The relevant texts that have survived are ancient and, despite the changes they may have undergone, provide information about the way of life and perceptions of people in the early stages of developed civilisation. Some references and descriptions show the importance of the thermal sense in shaping these texts and descriptions.

2.6.1. Ancient Greek and Roman Mythology and Tradition

Starting from Greek Mythology, the Elysian Fields (Figure 2) were part of the underworld. In this place, the souls of heroes and the virtuous found their final resting place. It is of great importance that this was the last residence, the place that would be the permanent home and where the soul would remain forever. These are described as meadows of flowers and trees where eternal spring prevailed. Under the shade of Myrtle (a Mediterranean plant), the virtuous and the heroes rode horseback and other athletic sports while playing music and other games. In the Odyssey, Homer says “Σοὶ δ᾽ οὐ θέσφατόν ἐστι, διοτρεφὲς ὦ Μενέλαε, Ἄργει ἐν ἱπποβότῳ θανέειν καὶ πότμον ἐπισπεῖν,ἀλλά σ᾽ ἐς Ἠλύσιον πεδίον καὶ πείρατα γαίης ἀθάνατοι πέμψουσιν, ὅθι ξανθὸς Ῥαδάμανθυς, τῇ περ ῥηΐστη βιοτὴ πέλει ἀνθρώποισιν οὐ νιφετός, οὔτ᾽ ἂρ χειμὼν πολὺς οὔτε ποτ᾽ ὄμβρος, ἀλλ᾽ αἰεὶ ζεφύροιο λιγὺ πνείοντος ἀήτας Ὠκεανὸς ἀνίησιν ἀναψύχειν ἀνθρώπους, οὕνεκ᾽ ἔχεις Ἑλένην καί σφιν γαμβρὸς Διός ἐσσι”, which means “as for you, divine Menelaus, it is not fated for you to close your eyes to Argos that feeds horses, and there find the fate of Death. To the ends of the earth, the gods will refer thee to the Elysian Fields, where the blond Rhodamante, where life blessed, graced, is coming of men. Snow does not fall, nor heavy winters, with showers unceasingly the ocean lifts the clear breaths of the zephyr and gives dew to men; you have Helen as your wife, you are the god of Dias-gamma, brother” [136,137]. We see that the Paradise of ancient Greek civilisation is a place that looks like a region without cold but with coolness and without extreme weather. Since ancient times, Greece’s region has had a warm climate with high sunshine duration [138,139,140,141]. Therefore, the inhabitants of this area did not want constant and prolonged exposure to heat and sun and would not want to be exposed to cold because they were not used to it. The Elysian Fields, the paradise of the ancient Greeks, the place where the virtuous and heroes would forever remain, is a place that ensures permanent thermal comfort. This is a place that will be thermally pleasant. Tartarus, which represents Hell according to Greek mythology (or ancient Greek religion), i.e., the place of eternal punishment, is described in detail by Virgil in the Aeneid. There he says that there is a river of fire called “Pyriphlegethon” and describes the area as a harvest that burns while wild winds stir up the flames. Tartarus is described as being in the depths of the Earth in caves. It was so deep that if one cast a bronze anvil, it would take 9 days and 9 nights to reach Tartarus [142,143]. That is, darkness and unbearable heat prevailed. On the one hand, Paradise was sunny but cool, while the Hell of the ancient Greeks was dark and hot. That is, we see that the place where those who deserved punishment would spend eternity had characteristics that the people of the Mediterranean region wanted to avoid, the unbearable heat and darkness. If we compare Paradise (Champs Élysées) and Hell (Tartarus), we can see that one of their main differences is the thermal sensation there. It is also crucial that both places will be the eternal dwelling place, which means that those who go there will live forever in these environments and the conditions they form. The conditions formed in these environments (Champs Élysées and Tartarus) are the reward and punishment, respectively. The imprint of the thermal sense in shaping the associated narratives is clear.

2.6.2. Ancient Egyptian Mythology and Tradition

In the region of Egypt and the surrounding areas, according to sources and analyses, high temperatures with extremely low rainfall have prevailed since the time of the Pharaohs. As a result, agriculture was based on the flooding of the Nile rather than on water from rainfall, which was insufficient [144,145,146]. According to the religion that prevailed in ancient Egypt, Hell (Duat) was a place with a vast element of fire, boiling water, and darkness. Like any place of punishment, it had demons that tormented those who reached it, but the environment was described as dark and extremely hot. In contrast, the Paradise of the ancient Egyptians (A’aru, Earu, or Iaru) was lush with meadows and plenty of water (Figure 3). In some depictions, it appears as a series of small islands occupied by reeds (rushes) [147,148]. As Brook–Hitching pinpointed [148], “this was the Paradise of the ancient Egyptian afterlife for all virtuous Egyptians, its lush, watered, green fields the very antipode of daily Egyptian life”; that is, Paradise had landscape characteristics that fostered humankind’s thermal sense and were the pleasant opposite of the everyday life of the ancient Egyptian. The eternal reward of a more pleasant afterlife is an environment of thermal comfort that was neither given nor common for the Egyptians of that time.

2.6.3. Northern Europe Ancient Mythology and Traditions

According to the mythologies and religions of the ancient peoples of the European North in the areas where the Vikings had spread, Hell was called Hel, a term related to the English term Hell referred to as a cold realm of shadow, where even its inhabitants were shivering. Many references to Hell in northern cultures place it in the frozen north, where famine was frequent [148,149,150]. The people who lived in northern Europe, i.e., Scandinavia and Iceland, suffered from a lack of food and the weather conditions of the northern European climate, which is cold and lacks sunshine. In this case, the connection between the place of eternal punishment and the conditions that shape the thermal environment of humankind is clear. Again, the northern regions’ climate elements that tormented them in their daily life are those mentioned in the sources describing their Hell. The Paradise of the northern peoples of that time was known as Valhalla, and, unlike what has been described so far in other cases, it was not an open space, but a huge building (hall) with hundreds of doors, and the roof was covered with hundreds of golden shields. This was where those who fell heroically in battle went. Those who got there would forever have plenty of good food and drink, and they could play sports or even fight (which was very popular at the time), and all wounds would be healed the next day [147,150,151]. Here, Paradise was a place without sun and shade, but it is a place protected from the weather. This difference is likely due to the nomadic life of the Vikings, who were constantly away from permanent homes as they travelled on their ships. Housing was lacking in their terrestrial life, as were the thermal conditions of a dwelling.

2.6.4. Islamic Religion and Tradition

The Arabian Peninsula, which is the region where the Islamic religion and tradition emerged and spread while experiencing a wide variety of climatic changes from the period of the emergence of this religion until today, has a dry and hot climate in a predominantly desert environment [152,153]. The inhabitants of this region of the planet were very often in extremely hot conditions (high temperature and low humidity and precipitation), regularly accompanied by high-intensity winds that even increased the loss of water (from the human body or from the environment). The Islamic tradition has its roots in the Arabian Peninsula, a region with a very hot and dry climate (desert). In this case, Hell, the place of eternal punishment, referred to as Jahannam or Gehenna, is a place with a fire that does not go out, and this is 69 times hotter than the fires of the Earth. The descriptions in many sacred texts of Islam describe a place of martyrdom dominated by fire. In other references, the existence of a great monster is described, which torments and threatens sinners who reach there [147,148,154].
In contrast, Paradise, the place where those who have lived virtuously and morally end up, is described as a beautiful garden with plenty of water, grass, and many large trees with flowers and fruit. The descriptions say that this beautiful garden even had carpets on the ground, as well as fine food and drink. There was also a regular northerly and cool wind that carried aromas [148,154,155]. In this case, we see an environment that forms thermal conditions that were desired by the inhabitants of these areas but were not common and usual in the areas where they spent their terrestrial life.

2.6.5. Jewish and Christianic Religion and Tradition

The area of present-day Israel and the surrounding areas has been dry with relatively high temperatures since ancient times. More specifically, the climate was cooler than that of neighbouring Egypt but warmer than that of the Greek area, and it had more rainfall than the Egyptian area but less than the Greek area [156,157,158,159]. Consequently, the inhabitants of the areas of present-day Israel very often experienced conditions of intense heat stress due to high temperatures and increased sunshine. Thus, in the case of the Jewish religion, things are less clear since there are two instances that seem to describe Hell. The first is Sheol, which is a dark set of caves where dust prevails [148,160,161]. Dust is another element of everyday life that bothered the inhabitants of the areas where the Jewish religion appeared and spread. The Sanctuaries report that Sheol was inside the Earth at great depth. The second is Gehenna (or Gehinnom), which, according to some reports, is a valley south of Jerusalem called Topheth where the ancient Canaanites made sacrifices to the gods Moloch and Baal. In later accounts of traditions, Gehenna is the place of Judgement, where the perpetual fire burns, burning the corpses of men and animals. Archaeologically no such place has been found in the valley south of Jerusalem [148,162,163,164]. The Paradise in the Jewish tradition is called Gan Eden and consists of five chambers; the first one is made of cedar, and the ceiling is made of transparent crystal. This room is the dwelling place of those who were not Jews but became devoted to this religion and code of life. The next is made of cedar, and the ceiling is covered with vine silver, which is the dwelling place of penitents. The third chamber is made of gold and silver and is very large, containing the best of Earth and Paradise with the most wonderful aromas, spices, and smells, with the huge Tree of Life in the centre. Under the shade of the Tree of Life are Abraham, Isaac, Jacob, and other iconic figures of the religion. The fourth chamber is made of olive wood and is inhabited by those who suffered for the name of their religion. According to Cohn-Sherbok [163], olives typify bitterness in taste and brilliancy in light (olive oil), symbolising persecution and its reward. The fifth chamber is built of precious stones, gold, and silver, surrounded by myrrh and aloes. In front of the chamber runs the river Gihon, on whose banks are planted shrubs affording perfume and aromatic incense. There are couches of gold and silver and fine drapery. This chamber is inhabited by the Messiah ben David, Elijah, and the Messiah of Ephraim (Joseph). In the centre is a canopy made of the cedars of Lebanon, in the style of the tabernacle, with posts and vessels of silver, and a settee of Lebanon wood with pillars of silver and a seat of gold, with a purple covering [163,164]. In contrast to the religious and mythological descriptions, in the case of the references to the Jewish religion, Paradise has no significant references that refer directly to factors that directly or indirectly shape the thermal environment.
The Christian religion appears after the Jewish religion in the same region, in the area of present-day Israel. The general climatic conditions of the region favoured heat stress from high temperatures and sunshine, and the inhabitants of the broader region suffered from it regularly as they were mainly farmers and herders. In the Christian tradition, according to Ekroth and Nilsson [142], “the representation of Hell was somewhat fixed in the imaginary of the Christian population of the Roman Empire. Its principal characteristics are darkness, stench, heat, and torment”. Moreover, the word “Hell” does not appear in the Greek New Testament; instead, one of three words is used: the Greek words Tartarus or Hades or the Hebrew word Gehinnom. Therefore, what details of these places does the New Testament give us? Matthew 5:22 warns of the “danger of Hell fire” as punishment, an “everlasting fire” that should be avoided at all costs: “And if thine eye offend thee, pluck it out, and cast it from thee: it is better for thee to enter into life with one eye, rather than having two eyes to be cast into Hell fire” (Matthew 18:9). In the blessing chanted during the funeral, it is stated that “Κύριε, ἀνάπαυσον τὴν ψυχὴν τοῦ κεκοιμημένου δούλου σου (τοῦδε), ἐν τόπῳ φωτεινῷ, ἐν τόπῳ χλοερῷ, ἐν τόπῳ ἀναψύξεως, ἔνθα ἀπέδρα ὀδύνη, λύπη καὶ στεναγμός”, which means “the Lord gave rest to the soul of the servants in a place of light, a place of grass and a place of dew, where there is no pain, sorrow, and sighing”. It becomes clear that the place where we would like every soul to go to stay is the place that is cool, with vegetation and light. This is the place that seems to have those characteristics that provide an environment of thermal comfort according to the needs of the early Christian peoples in the eastern Mediterranean.
It seems that Hell is related to extreme climate conditions, and Paradise is related to preferable and pleasant conditions mainly expressed by the thermal environment. Therefore, we see that the eternal reward and the reason for living according to the rules of one’s religious tradition is an excellent thermal environment. In contrast, the eternal punishment for not obeying the rules is an unpleasant thermal environment. The above reveals its (thermal environment and perception) central position in the value system of the societies of ancient civilisations.

3. Concluding Remarks

From the analysis of the basic parameters of human life in the first centuries of organised societies, it appears that the biometeorological and bioclimatic conditions, as the thermal environment shaped them, played a decisive, direct, and indirect role. More specifically, the following can be posited:
-
They largely determined the configuration of the outdoor and built spaces of humankind’s residential environment.
-
They have influenced and continue to control much of the amount of energy consumed by humankind, thus significantly affecting the economic model of our civilisation in every era.
-
They play an important role in the type of clothing since its inception as it is a fundamental tool for regulating the human body’s temperature.
-
They play a vital role in shaping human language and its sound according to prevalent climatic conditions.
-
They helped in the development of human socialisation and the development of democracy and philosophy.
-
They are at the core of the narrative of many religious beliefs and traditions, symbolising eternal punishment through Hell and reward through Heaven.
All the above shows a connection and influence of the thermal environment ranging from daily life issues to the perception of the afterlife.
Ultimately, the thermal sensation created by the bioclimatic and biometeorological environment is an underground, large, and powerful current that played and still plays a decisive role in the evolution of human civilisation by influencing every aspect of it.

Author Contributions

Conceptualisation, I.C. and A.M.; formal analysis I.C.; investigation, I.C.; resources, I.C.; writing—original draft preparation, I.C.; writing—review and editing, I.C. and A.M. All authors have read and agreed to the published version of the manuscript.

Funding

This research received no external funding.

Institutional Review Board Statement

Not applicable.

Informed Consent Statement

Not applicable.

Data Availability Statement

Not applicable.

Conflicts of Interest

The authors declare no conflict of interest.

References

  1. Ward, R. Climate and Man. Bull. Am. Geogr. Soc. 1907, 39, 735–738. [Google Scholar] [CrossRef]
  2. Olmstead, A.T. Climate and History. J. Geogr. 1912, 10, 163–168. [Google Scholar] [CrossRef]
  3. Böhme, G. Atmosphere. Online Encycl. Philos. Nat. 2021. [Google Scholar] [CrossRef]
  4. Ward, P. Out of Thin Air: Dinosaurs, Birds, and Earth’s Ancient Atmosphere; Joseph Henry Press: Washington, DC, USA, 2006; ISBN 978-0-30910-061-8. [Google Scholar]
  5. Böhme, G.; Thibaud, J.-P. The Aesthetics of Atmospheres; Routledge: London, UK, 2016; ISBN 978-1-13868-850-6. [Google Scholar]
  6. Pfister, D. The Concept of Atmosphere from a Multidisciplinary Perspective. In Atmospheric Turn in Culture and Tourism: Place, Design and Process Impacts on Customer Behaviour, Marketing and Branding; Volgger, M., Pfister, D., Eds.; Advances in Culture, Tourism and Hospitality Research; Emerald Publishing Limited: Bingley, UK, 2019; Volume 16, pp. 31–43. ISBN 978-1-83867-070-2. [Google Scholar]
  7. Bonacina, L.C.W. Landscape Meteorology and Its Reflection in Art and Literature. Q. J. R. Meteorol. Soc. 1939, 65, 485–498. [Google Scholar] [CrossRef]
  8. Neuberger, H. Climate in Art. Weather 1970, 25, 46–56. [Google Scholar] [CrossRef]
  9. Lai, D.; Lian, Z.; Liu, W.; Guo, C.; Liu, W.; Liu, K.; Chen, Q. A Comprehensive Review of Thermal Comfort Studies in Urban Open Spaces. Sci. Total Environ. 2020, 742, 140092. [Google Scholar] [CrossRef]
  10. Givoni, B. Comfort, Climate Analysis and Building Design Guidelines. Energy Build. 1992, 18, 11–23. [Google Scholar] [CrossRef]
  11. Lamb, H. Climate, History and the Modern World; Routledge: New York, NY, USA, 1997. [Google Scholar]
  12. Donaldson, G.C.; Rintamäki, H.; Näyhä, S. Outdoor Clothing: Its Relationship to Geography, Climate, Behaviour and Cold-Related Mortality in Europe. Int. J. Biometeorol. 2001, 45, 45–51. [Google Scholar] [CrossRef]
  13. Tamura, T. Climate and Clothing. J. Hum.-Environ. Syst. 2016, 19, 1–11. [Google Scholar] [CrossRef] [Green Version]
  14. Huntington, E. Mainsprings of Civilization; Wiley: Hoboken, NJ, USA, 1945. [Google Scholar]
  15. Doxiadis, C.A. Man’s Movement and His Settlements? Int. J. Environ. Stud. 1970, 1, 19–30. [Google Scholar] [CrossRef]
  16. Ingram, M.J.; Underhill, D.J.; Wigley, T.M.L. Historical Climatology. Nature 1978, 276, 329–334. [Google Scholar] [CrossRef]
  17. Hippocrates On Airs, Waters and Places; Dodo Press: Moscow, Russia, 2009; ISBN 978-1-40994-959-6.
  18. Parsons, K. Human Thermal Environments: The Effects of Hot, Moderate, and Cold Environments on Human Health, Comfort, and Performance, 3rd ed.; CRC Press, Taylor & Francis Group: Boca Raton, FL, USA, 2002; ISBN 1-46-659599-X. [Google Scholar]
  19. McGregor, G.R. Human Biometeorology. Prog. Phys. Geogr. Earth Environ. 2012, 36, 93–109. [Google Scholar] [CrossRef]
  20. Bouma, J.J.S.H.J.W. A Short History of Human Biometeorology. Experientia 1987, 43, 2–6. [Google Scholar] [CrossRef]
  21. Winslow, C.-E.A.; Herrington, L.P.; Gagge, A.P. Physiological Reactions of the Human Body to Varying Environmental Temperatures. Am. J. Physiol. Leg. Content 1937, 120, 1–22. [Google Scholar] [CrossRef] [Green Version]
  22. Gagge, A.P.; Stolwijk, J.A.J.; Hardy, J.D. Comfort and Thermal Sensations and Associated Physiological Responses at Various Ambient Temperatures. Environ. Res. 1967, 1, 1–20. [Google Scholar] [CrossRef]
  23. Auliciems, A. Towards a Psycho-Physiological Model of Thermal Perception. Int. J. Biometeorol. 1981, 25, 109–122. [Google Scholar] [CrossRef]
  24. Djongyang, N.; Tchinda, R.; Njomo, D. Thermal Comfort: A Review Paper. Renew. Sustain. Energy Rev. 2010, 14, 2626–2640. [Google Scholar] [CrossRef]
  25. Cena, K.; Clark, J.A. Bioengineering, Thermal Physiology and Comfort; Elsevier: Amsterdam, The Netherlands, 1981; Volume 10, ISBN 0-08-087469-X. [Google Scholar]
  26. Griffiths, I.D.; Boyce, P.R. Performance and Thermal Comfort. Ergonomics 1971, 14, 457–468. [Google Scholar] [CrossRef]
  27. Potchter, O.; Cohen, P.; Lin, T.-P.; Matzarakis, A. Outdoor Human Thermal Perception in Various Climates: A Comprehensive Review of Approaches, Methods and Quantification. Sci. Total Environ. 2018, 631–632, 390–406. [Google Scholar] [CrossRef]
  28. de Freitas, C.R.; Grigorieva, E.A. A Comprehensive Catalogue and Classification of Human Thermal Climate Indices. Int. J. Biometeorol. 2015, 59, 109–120. [Google Scholar] [CrossRef]
  29. Charalampopoulos, I. The R Language as a Tool for Biometeorological Research. Atmosphere 2020, 11, 682. [Google Scholar] [CrossRef]
  30. Matzarakis, A.; Mayer, H.; Iziomon, M.G. Applications of a Universal Thermal Index: Physiological Equivalent Temperature. Int. J. Biometeorol. 1999, 43, 76–84. [Google Scholar] [CrossRef] [PubMed]
  31. Nouri, A.S.; Charalampopoulos, I.; Matzarakis, A. Beyond Singular Climatic Variables—Identifying the Dynamics of Wholesome Thermo-Physiological Factors for Existing/Future Human Thermal Comfort during Hot Dry Mediterranean Summers. Int. J. Environ. Res. Public Health 2018, 15, 2362. [Google Scholar] [CrossRef] [PubMed] [Green Version]
  32. Charalampopoulos, I. A Comparative Sensitivity Analysis of Human Thermal Comfort Indices with Generalized Additive Models. Theor. Appl. Clim. 2019, 137, 1605–1622. [Google Scholar] [CrossRef]
  33. Zafarmandi, S.; Mahdavinejad, M.; Norford, L.; Matzarakis, A. Analyzing Thermal Comfort Sensations in Semi-Outdoor Space on a University Campus: On-Site Measurements in Tehran’s Hot and Cold Seasons. Atmosphere 2022, 13, 1034. [Google Scholar] [CrossRef]
  34. Paramita, B.; Kusuma, H.E.; Matzarakis, A. Urban Performance Based on Biometeorology Index in High-Density, Hot, and Humid Cities. Sustain. Cities Soc. 2022, 80, 103767. [Google Scholar] [CrossRef]
  35. Nouri, A.S.; Charalampopoulos, I.; Matzarakis, A. The Application of the Physiologically Equivalent Temperature to Determine Impacts of Locally Defined Extreme Heat Events within Vulnerable Dwellings during the 2020 Summer in Ankara: Abstract. Sustain. Cities Soc. 2022, 81, 103833. [Google Scholar] [CrossRef]
  36. Matzarakis, A.; Graw, K. Human Bioclimate Analysis for the Paris Olympic Games. Atmosphere 2022, 13, 269. [Google Scholar] [CrossRef]
  37. Krüger, E.L. Literature Review on UTCI Applications. In Applications of the Universal Thermal Climate Index UTCI in Biometeorology: Latest Developments and Case Studies; Krüger, E.L., Ed.; Biometeorology; Springer International Publishing: Cham, Switzerland, 2021; pp. 23–65. ISBN 978-3-03076-716-7. [Google Scholar]
  38. Aplin, K.L.; Williams, P.D. Meteorological Phenomena in Western Classical Orchestral Music. Weather 2011, 66, 300–306. [Google Scholar] [CrossRef] [Green Version]
  39. Brown, S.; Aplin, K.L.; Jenkins, K.; Mander, S.; Walsh, C.; Williams, P.D. Is There a Rhythm of The Rain? An Analysis of Weather in Popular Music. Weather 2015, 70, 198–204. [Google Scholar] [CrossRef]
  40. deMenocal, P.B. Cultural Responses to Climate Change During the Late Holocene. Science 2001, 292, 667–673. [Google Scholar] [CrossRef]
  41. Thornes, J.E. Cultural Climatology and the Representation of Sky, Atmosphere, Weather and Climate in Selected Art Works of Constable, Monet and Eliasson. Geoforum 2008, 39, 570–580. [Google Scholar] [CrossRef]
  42. Minor, K.; Bjerre-Nielsen, A.; Jonasdottir, S.S.; Lehmann, S.; Obradovich, N. Rising Temperatures Erode Human Sleep Globally. One Earth 2022, 5, 534–549. [Google Scholar] [CrossRef]
  43. Lai, W.; Li, S.; Liu, Y.; Barwick, P.J. Adaptation Mitigates the Negative Effect of Temperature Shocks on Household Consumption. Nat. Hum. Behav. 2022, 6, 837–846. [Google Scholar] [CrossRef]
  44. Trentinaglia, M.T.; Parolini, M.; Donzelli, F.; Olper, A. Climate Change and Obesity: A Global Analysis. Glob. Food Secur. 2021, 29, 100539. [Google Scholar] [CrossRef]
  45. de Lima, C.Z.; Buzan, J.R.; Moore, F.C.; Baldos, U.L.C.; Huber, M.; Hertel, T.W. Heat Stress on Agricultural Workers Exacerbates Crop Impacts of Climate Change. Environ. Res. Lett. 2021, 16, 044020. [Google Scholar] [CrossRef]
  46. Beghin, L.; Vanhelst, J.; Drumez, E.; Migueles, J.; Manios, Y.; Moreno, L.A.; Henauw, S.D.; Gottrand, F. Influence of Meteorological Conditions on Physical Activity in Adolescents. J. Epidemiol. Community Health 2020, 74, 395–400. [Google Scholar] [CrossRef]
  47. Mullins, J.T.; White, C. Temperature and Mental Health: Evidence from the Spectrum of Mental Health Outcomes. J. Health Econ. 2019, 68, 102240. [Google Scholar] [CrossRef] [Green Version]
  48. Obradovich, N.; Migliorini, R.; Paulus, M.P.; Rahwan, I. Empirical Evidence of Mental Health Risks Posed by Climate Change. Proc. Natl. Acad. Sci. USA 2018, 115, 10953–10958. [Google Scholar] [CrossRef] [Green Version]
  49. Charalampopoulos, I.; Droulia, F. The Agro-Meteorological Caused Famines as an Evolutionary Factor in the Formation of Civilisation and History: Representative Cases in Europe. Climate 2021, 9, 5. [Google Scholar] [CrossRef]
  50. Tsonis, A.A.; Swanson, K.L.; Sugihara, G.; Tsonis, P.A. Climate Change and the Demise of Minoan Civilization. Clim. Past 2010, 6, 525–530. [Google Scholar] [CrossRef] [Green Version]
  51. Fagan, B.M. Floods, Famines, and Emperors: El Niño and the Fate of Civilizations, 2nd ed.; Basic Books: New York, NY, USA, 2009; ISBN 978-0-46500-530-7. [Google Scholar]
  52. Haug, G.H.; Günther, D.; Peterson, L.C.; Sigman, D.M.; Hughen, K.A.; Aeschlimann, B. Climate and the Collapse of Maya Civilization. Science 2003, 299, 1731–1735. [Google Scholar] [CrossRef] [PubMed]
  53. Hodell, D.A.; Curtis, J.H.; Brenner, M. Possible Role of Climate in the Collapse of Classic Maya Civilization. Nature 1995, 375, 391–394. [Google Scholar] [CrossRef]
  54. Abate, T. Climate and the Collapse of Civilization. BioScience 1994, 44, 516–519. [Google Scholar] [CrossRef]
  55. Neumann, J. Great Historical Events That Were Significantly Affected by the Weather: I. the Mongol Invasions of Japan. Bull. Am. Meteorol. Soc. 1975, 56, 1167–1171. [Google Scholar] [CrossRef]
  56. Neumann, J.; Dettwiller, J. Great Historical Events That Were Significantly Affected by the Weather: Part 9, the Year Leading to the Revolution of 1789 in France (II). Bull. Am. Meteorol. Soc. 1990, 71, 33–41. [Google Scholar] [CrossRef]
  57. Lindgrén, S.; Neumann, J. Great Historical Events That Were Significantly Affected by the Weather: 5, Some Meteorological Events of the Crimean War and Their Consequences. Bull. Am. Meteor. Soc. 1980, 61, 1570–1583. [Google Scholar] [CrossRef]
  58. Klinger, P.J. Weather and the Jacobite Rebellion of 1719. Environ. Hist. 2017, 23, 197–216. [Google Scholar] [CrossRef]
  59. Grove, R.H. The Great El Niño of 1789–93 and Its Global Consequences: Reconstructing an Extreme Climate Event in World Environmental History. Mediev. Hist. J. 2006, 10, 75–98. [Google Scholar] [CrossRef]
  60. Santos Nouri, A.; Çalışkan, O.; Charalampopoulos, I.; Cheval, S.; Matzarakis, A. Defining Local Extreme Heat Thresholds and Indoor Cooling Degree Necessity for Vulnerable Residential Dwellings during the 2020 Summer in Ankara—Part I: Air Temperature. Sol. Energy 2021, 242, 435–453. [Google Scholar] [CrossRef]
  61. Santurtún, A.; Almendra, R.; Fdez-Arroyabe, P.; Sanchez-Lorenzo, A.; Royé, D.; Zarrabeitia, M.T.; Santana, P. Predictive Value of Three Thermal Comfort Indices in Low Temperatures on Cardiovascular Morbidity in the Iberian Peninsula. Sci. Total Environ. 2020, 729, 138969. [Google Scholar] [CrossRef]
  62. Nouri, A.S.; Matzarakis, A. Human Biometeorological Models: Existing and Future Reflections for Lisbon. In Urban Microclimate Modelling for Comfort and Energy Studies; Palme, M., Salvati, A., Eds.; Springer International Publishing: Cham, Switzerland, 2021; pp. 443–464. ISBN 978-3-03065-421-4. [Google Scholar]
  63. Nouri, A.S.; Lopes, A.; Costa, J.P.; Matzarakis, A. Confronting Potential Future Augmentations of the Physiologically Equivalent Temperature through Public Space Design: The Case of Rossio, Lisbon. Sustain. Cities Soc. 2018, 37, 7–25. [Google Scholar] [CrossRef]
  64. Watts, N.; Amann, M.; Arnell, N.; Ayeb-Karlsson, S.; Beagley, J.; Belesova, K.; Boykoff, M.; Byass, P.; Cai, W.; Campbell-Lendrum, D.; et al. The 2020 Report of The Lancet Countdown on Health and Climate Change: Responding to Converging Crises. Lancet 2021, 397, 129–170. [Google Scholar] [CrossRef]
  65. Yi, W.; Zhao, Y.; Chan, A.P.C.; Lam, E.W.M. Optimal Cooling Intervention for Construction Workers in a Hot and Humid Environment. Build. Environ. 2017, 118, 91–100. [Google Scholar] [CrossRef]
  66. Ebi, K.L.; Capon, A.; Berry, P.; Broderick, C.; de Dear, R.; Havenith, G.; Honda, Y.; Kovats, R.S.; Ma, W.; Malik, A.; et al. Hot Weather and Heat Extremes: Health Risks. Lancet 2021, 398, 698–708. [Google Scholar] [CrossRef]
  67. Chen, A.; Chang, V.W.-C. Human Health and Thermal Comfort of Office Workers in Singapore. Build. Environ. 2012, 58, 172–178. [Google Scholar] [CrossRef]
  68. Obradovich, N.; Migliorini, R. Sleep and the Human Impacts of Climate Change. Sleep Med. Rev. 2018, 42, 1–2. [Google Scholar] [CrossRef]
  69. Obradovich, N.; Migliorini, R.; Mednick, S.C.; Fowler, J.H. Nighttime Temperature and Human Sleep Loss in a Changing Climate. Sci. Adv. 2017, 3, e1601555. [Google Scholar] [CrossRef] [Green Version]
  70. Matzarakis, A.; Mayer, H. The Extreme Heat Wave in Athens in July 1987 from the Point of View of Human Biometeorology. Atmos. Environ. Part B Urban Atmos. 1991, 25, 203–211. [Google Scholar] [CrossRef]
  71. Buyak, N.A.; Deshko, V.I.; Sukhodub, I.O. Buildings Energy Use and Human Thermal Comfort According to Energy and Exergy Approach. Energy Build. 2017, 146, 172–181. [Google Scholar] [CrossRef]
  72. Yang, L.; Yan, H.; Lam, J.C. Thermal Comfort and Building Energy Consumption Implications—A Review. Appl. Energy 2014, 115, 164–173. [Google Scholar] [CrossRef]
  73. Halawa, E.; van Hoof, J.; Soebarto, V. The Impacts of the Thermal Radiation Field on Thermal Comfort, Energy Consumption and Control—A Critical Overview. Renew. Sustain. Energy Rev. 2014, 37, 907–918. [Google Scholar] [CrossRef]
  74. Charalampopoulos, I.; Santos Nouri, A. Investigating the Behaviour of Human Thermal Indices under Divergent Atmospheric Conditions: A Sensitivity Analysis Approach. Atmosphere 2019, 10, 580. [Google Scholar] [CrossRef] [Green Version]
  75. Labdaoui, K.; Mazouz, S.; Acidi, A.; Cools, M.; Moeinaddini, M.; Teller, J. Utilizing Thermal Comfort and Walking Facilities to Propose a Comfort Walkability Index (CWI) at the Neighbourhood Level. Build. Environ. 2021, 193, 107627. [Google Scholar] [CrossRef]
  76. Lin, T.-P.; Yang, S.-R.; Chen, Y.-C.; Matzarakis, A. The Potential of a Modified Physiologically Equivalent Temperature (MPET) Based on Local Thermal Comfort Perception in Hot and Humid Regions. Theor. Appl. Clim. 2019, 135, 873–876. [Google Scholar] [CrossRef]
  77. Jendritzky, G.; de Dear, R.; Havenith, G. UTCI—Why Another Thermal Index? Int. J. Biometeorol. 2012, 56, 421–428. [Google Scholar] [CrossRef] [Green Version]
  78. Orosa, J.A.; Oliveira, A.C. A New Thermal Comfort Approach Comparing Adaptive and PMV Models. Renew. Energy 2011, 36, 951–956. [Google Scholar] [CrossRef]
  79. Charalampopoulos, I.; Tsiros, I.; Chronopoulou-Sereli, A.; Matzarakis, A. A Methodology for the Evaluation of the Human-Bioclimatic Performance of Open Spaces. Theor. Appl. Clim. 2017, 128, 811–820. [Google Scholar] [CrossRef]
  80. Matzarakis, A.; Rutz, F.; Mayer, H. Modelling Radiation Fluxes in Simple and Complex Environments—Application of the RayMan Model. Int. J. Biometeorol. 2007, 51, 323–334. [Google Scholar] [CrossRef]
  81. Nastos, P.T.; Vassilakis, E.; Nastos, M.-P.P.; Charalampopoulos, I.; Matzarakis, A. Assessment of Continuous Sky View Factor Based on Ultra-High Resolution Natural Colour Images Acquired by Remotely Piloted Airborne Systems for Applications in an Urban Area of Athens. Int. J. Remote Sens. 2017, 38, 5814–5829. [Google Scholar] [CrossRef]
  82. Nastos, P.T.; Matzarakis, A. The Effect of Air Temperature and Human Thermal Indices on Mortality in Athens, Greece. Theor. Appl. Clim. 2012, 108, 591–599. [Google Scholar] [CrossRef]
  83. Harari, Y.N. Sapiens: A Brief History of Humankind; Random House: New York, NY, USA, 2014; ISBN 1-84-655823-9. [Google Scholar]
  84. Pevsner, N. A History of Building Types; Thames and Hudson: London, UK, 1976; Volume 19, ISBN 0-50-034066-8. [Google Scholar]
  85. Bowen, W.M.; Gleeson, R.E. The Evolution of Human Settlements: From Pleistocene Origins to Anthropocene Prospects; Springer: Berlin/Heidelberg, Germany, 2018; ISBN 978-3-31995-033-4. [Google Scholar]
  86. Day, C.; Roaf, S. Ecohouse: A Design Guide; Routledge: London, UK, 2007; ISBN 978-0-41552-677-7. [Google Scholar]
  87. Brown, R. Design with Microclimate. The Secret to Comfortable Outdoor Space; Island Press: Washington, DC, USA, 2010. [Google Scholar]
  88. Diamond, J. Guns, Germs, and Steel: The Fates of Human Societies; WW Norton & Company: New York, NY, USA, 1999; ISBN 0-39-306922-2. [Google Scholar]
  89. Manzano-Agugliaro, F.; Montoya, F.G.; Sabio-Ortega, A.; García-Cruz, A. Review of Bioclimatic Architecture Strategies for Achieving Thermal Comfort. Renew. Sustain. Energy Rev. 2015, 49, 736–755. [Google Scholar] [CrossRef]
  90. Rodríguez Algeciras, J.A.; Coch, H.; De la Paz Pérez, G.; Chaos Yeras, M.; Matzarakis, A. Human Thermal Comfort Conditions and Urban Planning in Hot-Humid Climates—The Case of Cuba. Int. J. Biometeorol. 2016, 60, 1151–1164. [Google Scholar] [CrossRef]
  91. Mohamed, A.S.Y.; Elmeligy, D.A.; Azmy, N.Y. Eco-Adaptive Architecture through the Bioclimatic Design in Historical Arab Regions. EQA Int. J. Environ. Qual. 2020, 39, 32–51. [Google Scholar] [CrossRef]
  92. Tamaskani Esfehankalateh, A.; Farrokhzad, M.; Tamaskani Esfehankalateh, F.; Soflaei, F. Bioclimatic Passive Design Strategies of Traditional Houses in Cold Climate Regions. Environ. Dev. Sustain. 2022, 24, 10027–10068. [Google Scholar] [CrossRef]
  93. Karjalainen, S. Thermal Comfort and Gender: A Literature Review. Indoor Air 2012, 22, 96–109. [Google Scholar] [CrossRef]
  94. Lin, T.-P. Thermal Perception, Adaptation and Attendance in a Public Square in Hot and Humid Regions. Build. Environ. 2009, 44, 2017–2026. [Google Scholar] [CrossRef]
  95. Parsons, K.C. The Effects of Gender, Acclimation State, the Opportunity to Adjust Clothing and Physical Disability on Requirements for Thermal Comfort. Energy Build. 2002, 34, 593–599. [Google Scholar] [CrossRef]
  96. Charalampopoulos, I.; Nastos, P.T.; Didaskalou, E. Human Thermal Conditions and North Europeans’ Web Searching Behavior (Google Trends) on Mediterranean Touristic Destinations. Urban Sci. 2017, 1, 8. [Google Scholar] [CrossRef] [Green Version]
  97. Fanger, P.O. Thermal Comfort: Analysis and Applications in Environmental Engineering; McGraw-Hill Book Company: New York, NY, USA, 1970; ISBN 978-0-07019-915-6. [Google Scholar]
  98. Chatzipoulka, C.; Steemers, K.; Nikolopoulou, M. Density and Coverage Values as Indicators of Thermal Diversity in Open Spaces: Comparative Analysis of London and Paris Based on Sun and Wind Shadow Maps. Cities 2020, 100, 102645. [Google Scholar] [CrossRef]
  99. Nouri, A.S.; Costa, J.P. Addressing Thermophysiological Thresholds and Psychological Aspects during Hot and Dry Mediterranean Summers through Public Space Design: The Case of Rossio. Build. Environ. 2017, 118, 67–90. [Google Scholar] [CrossRef]
  100. Yang, S.-Q.; Matzarakis, A. Implementation of Human Thermal Comfort Information in Köppen-Geiger Climate Classification—The Example of China. Int. J. Biometeorol. 2016, 60, 1801–1805. [Google Scholar] [CrossRef] [PubMed]
  101. Charalampopoulos, I.; Tsiros, I.; Chronopoulou-Sereli, A.; Matzarakis, A. A Note on the Evolution of the Daily Pattern of Thermal Comfort-Related Micrometeorological Parameters in Small Urban Sites in Athens. Int. J. Biometeorol. 2014, 59, 1223–1236. [Google Scholar] [CrossRef] [PubMed]
  102. Kabre, C. Sustainable Greek Traditional Dwellings of Cyclades. Archit. Sci. Rev. 2016, 59, 81–90. [Google Scholar] [CrossRef]
  103. Nastos, P.T.; Matzarakis, A. Present and Future Climate—Tourism Conditions in Milos Island, Greece. Atmosphere 2019, 10, 145. [Google Scholar] [CrossRef] [Green Version]
  104. Aljawabra, F.; Nikolopoulou, M. Influence of Hot Arid Climate on the Use of Outdoor Urban Spaces and Thermal Comfort: Do Cultural and Social Backgrounds Matter? Intell. Build. Int. 2010, 2, 198–217. [Google Scholar] [CrossRef]
  105. Bouden, C.; Ghrab, N. An Adaptive Thermal Comfort Model for the Tunisian Context: A Field Study Results. Energy Build. 2005, 37, 952–963. [Google Scholar] [CrossRef]
  106. Andreou, E.; Axarli, K. Investigation of Urban Canyon Microclimate in Traditional and Contemporary Environment. Experimental Investigation and Parametric Analysis. Renew. Energy 2012, 43, 354–363. [Google Scholar] [CrossRef]
  107. Lindberg, F.; Thorsson, S.; Rayner, D.; Lau, K. The Impact of Urban Planning Strategies on Heat Stress in a Climate-Change Perspective. Sustain. Cities Soc. 2016, 25, 1–12. [Google Scholar] [CrossRef]
  108. Svensson, M.K.; Eliasson, I. Diurnal Air Temperatures in Built-up Areas in Relation to Urban Planning. Landsc. Urban Plan. 2002, 61, 37–54. [Google Scholar] [CrossRef]
  109. Nikolopoulou, M.; Steemers, K. Thermal Comfort and Psychological Adaptation as a Guide for Designing Urban Spaces. Energy Build. 2003, 35, 95–101. [Google Scholar] [CrossRef]
  110. Yang, B.; Olofsson, T.; Nair, G.; Kabanshi, A. Outdoor Thermal Comfort under Subarctic Climate of North Sweden—A Pilot Study in Umeå. Sustain. Cities Soc. 2017, 28, 387–397. [Google Scholar] [CrossRef]
  111. Kim, Y.J.; Brown, R.D. A Multilevel Approach for Assessing the Effects of Microclimatic Urban Design on Pedestrian Thermal Comfort: The High Line in New York. Build. Environ. 2021, 205, 108244. [Google Scholar] [CrossRef]
  112. Smil, V. Energy and Civilization: A History; MIT Press: Cambridge, MA, USA, 2018; ISBN 978-0-26253-616-5. [Google Scholar]
  113. Issawi, C. Technology, Energy, and Civilization: Some Historical Observations. Int. J. Middle East Stud. 1991, 23, 281–289. [Google Scholar] [CrossRef]
  114. Albatayneh, A.; Alterman, D.; Page, A.; Moghtaderi, B. The Impact of the Thermal Comfort Models on the Prediction of Building Energy Consumption. Sustainability 2018, 10, 3609. [Google Scholar] [CrossRef] [Green Version]
  115. Jowkar, M.; Rijal, H.B.; Montazami, A.; Brusey, J.; Temeljotov-Salaj, A. The Influence of Acclimatization, Age and Gender-Related Differences on Thermal Perception in University Buildings: Case Studies in Scotland and England. Build. Environ. 2020, 179, 106933. [Google Scholar] [CrossRef]
  116. Vellei, M.; Chinazzo, G.; Zitting, K.-M.; Hubbard, J. Human Thermal Perception and Time of Day: A Review. Temperature 2021, 8, 320–341. [Google Scholar] [CrossRef]
  117. Ross, R. Clothing: A Global History; Polity: Cambridge, UK, 2008; ISBN 978-0-74563-186-8. [Google Scholar]
  118. Gao, S.; Ooka, R.; Oh, W. Experimental Investigation of the Effect of Clothing Insulation on Thermal Comfort Indices. Build. Environ. 2021, 187, 107393. [Google Scholar] [CrossRef]
  119. Jowkar, M.; de Dear, R.; Brusey, J. Influence of Long-Term Thermal History on Thermal Comfort and Preference. Energy Build. 2020, 210, 109685. [Google Scholar] [CrossRef]
  120. Gautam, B.; Rijal, H.B.; Shukuya, M.; Imagawa, H. A Field Investigation on the Wintry Thermal Comfort and Clothing Adjustment of Residents in Traditional Nepalese Houses. J. Build. Eng. 2019, 26, 100886. [Google Scholar] [CrossRef]
  121. Sahta, I.; Baltina, I.; Blums, J.; Jurkans, V. The Control of Human Thermal Comfort by the Smart Clothing. SHS Web Conf. 2014, 10, 00040. [Google Scholar] [CrossRef] [Green Version]
  122. Havenith, G.; Holmér, I.; Parsons, K. Personal Factors in Thermal Comfort Assessment: Clothing Properties and Metabolic Heat Production. Energy Build. 2002, 34, 581–591. [Google Scholar] [CrossRef]
  123. Nölle, J.; Fusaroli, R.; Mills, G.J.; Tylén, K. Language as Shaped by the Environment: Linguistic Construal in a Collaborative Spatial Task. Palgrave Commun 2020, 6, 27. [Google Scholar] [CrossRef] [Green Version]
  124. Everett, C.; Blasi, D.E.; Roberts, S.G. Climate, Vocal Folds, and Tonal Languages: Connecting the Physiological and Geographic Dots. Proc. Natl. Acad. Sci. USA 2015, 112, 1322–1327. [Google Scholar] [CrossRef] [PubMed] [Green Version]
  125. Maddieson, I. Language Adapts to Environment: Sonority and Temperature. Front. Commun. 2018, 3, 28. [Google Scholar] [CrossRef] [Green Version]
  126. Everett, C.; Blasí, D.E.; Roberts, S.G. Language Evolution and Climate: The Case of Desiccation and Tone. J. Lang. Evol. 2016, 1, 33–46. [Google Scholar] [CrossRef]
  127. Gorenflo, L.J.; Romaine, S.; Mittermeier, R.A.; Walker-Painemilla, K. Co-Occurrence of Linguistic and Biological Diversity in Biodiversity Hotspots and High Biodiversity Wilderness Areas. Proc. Natl. Acad. Sci. USA 2012, 109, 8032–8037. [Google Scholar] [CrossRef] [Green Version]
  128. Maddieson, I.; Coupé, C. Human Spoken Language Diversity and the Acoustic Adaptation Hypothesis. J. Acoust. Soc. Am. 2015, 138, 1838. [Google Scholar] [CrossRef]
  129. Mariak, Z.; White, M.D.; Lewko, J.; Lyson, T.; Piekarski, P. Direct Cooling of the Human Brain by Heat Loss from the Upper Respiratory Tract. J. Appl. Physiol. 1999, 87, 1609–1613. [Google Scholar] [CrossRef]
  130. Naddaf, G. The Greek Concept of Nature; State University of New York Press: Albany, NY, USA, 2005; ISBN 978-0-79146-374-1. [Google Scholar]
  131. Roochnik, D. Retrieving the Ancients: An Introduction to Greek Philosophy; Wiley: Hoboken, NJ, US, 2004; ISBN 978-1-40510-862-1. [Google Scholar]
  132. Baltes, M. Plato’s School, the Academy. Hermathena 1993, 5–26. [Google Scholar]
  133. Luce, J.V. An Introduction to Greek Philosophy; Thames and Hudson: London, UK, 1992; ISBN 978-0-50027-655-6. [Google Scholar]
  134. Gottschalk, H.B. Notes on the Wills of the Peripatetic Scholarchs. Hermes 1972, 100, 314–342. [Google Scholar]
  135. Cohen, S.M.; Curd, P.; Reeve, C.D.C. Readings in Ancient Greek Philosophy: From Thales to Aristotle; Hackett Publishing: Indianapolis, IN, USA, 2016; ISBN 978-1-62466-534-9. [Google Scholar]
  136. Anderson, W.S. Calypso and Elysium. Class. J. 1958, 54, 2–11. [Google Scholar]
  137. Kearns, E. Elysium. Available online: https://oxfordre.com/classics/view/10.1093/acrefore/9780199381135.001.0001/acrefore-9780199381135-e-2390 (accessed on 29 August 2022).
  138. Zarkadoulas, N.; Koutsoyiannis, D.; Mamassis, N.; Papalexiou, S.M. Climate, Water and Health in Ancient Greece; European Geosciences Union: Munich, Germany, 2008. [Google Scholar]
  139. Runnels, C.N. Environmental Degradation in Ancient Greece. Sci. Am. 1995, 272, 96–99. [Google Scholar] [CrossRef]
  140. Knitter, D.; Günther, G.; Hamer, W.B.; Keßler, T.; Seguin, J.; Unkel, I.; Weiberg, E.; Duttmann, R.; Nakoinz, O. Land Use Patterns and Climate Change—a Modeled Scenario of the Late Bronze Age in Southern Greece. Environ. Res. Lett. 2019, 14, 125003. [Google Scholar] [CrossRef] [Green Version]
  141. Okuda, M.; Yasuda, Y.; Setoguchi, T. Middle to Late Pleistocene Vegetation History and Climatic Changes at Lake Kopais, Southeast Greece. Boreas 2001, 30, 73–82. [Google Scholar] [CrossRef]
  142. Ekroth, G.; Nilsson, I. Round Trip to Hades in the Eastern Mediterranean Tradition: Visits to the Underworld from Antiquity to Byzantium; BRILL: Leiden, The Netherlands, 2018; ISBN 978-9-00437-596-3. [Google Scholar]
  143. Lye, S. The Goddess Styx and the Mapping of World Order in Hesiod’s “Theogony”. Rev. Philos. Anc. 2009, 27, 3–31. [Google Scholar]
  144. Bell, B. The Dark Ages in Ancient History. I. The First Dark Age in Egypt. Am. J. Archaeol. 1971, 75, 1–26. [Google Scholar] [CrossRef] [Green Version]
  145. Welc, F.; Marks, L. Climate Change at the End of the Old Kingdom in Egypt around 4200 BP: New Geoarchaeological Evidence. Quat. Int. 2014, 324, 124–133. [Google Scholar] [CrossRef]
  146. Lionello, P. The Climate of the Mediterranean Region: From the Past to the Future; Elsevier: Amsterdam, The Netherlands, 2012; ISBN 978-0-12416-042-2. [Google Scholar]
  147. Casey, J. After Lives: A Guide to Heaven, Hell, and Purgatory; Illustrated edition; Oxford University Press: Oxford, UK, 2009; ISBN 978-0-19509-295-0. [Google Scholar]
  148. Brooke-Hitching, E. The Devil’s Atlas: An Explorer’s Guide to Heavens, Hells and Afterworlds; Chronicle Books: London, UK, 2022; ISBN 978-1-79721-447-4. [Google Scholar]
  149. Price, N. Nine Paces from Hel: Time and Motion in Old Norse Ritual Performance. World Archaeol. 2014, 46, 178–191. [Google Scholar] [CrossRef]
  150. Carlsen, C. Old Norse Visions of the Afterlife. Oxford University Press: Oxford, UK, 2012. [Google Scholar]
  151. O’Donoghue, H. From Asgard to Valhalla: The Remarkable History of the Norse Myths; Bloomsbury Publishing: London, UK, 2007; ISBN 1-84-511829-4. [Google Scholar]
  152. Petraglia, M.D.; Groucutt, H.S.; Guagnin, M.; Breeze, P.S.; Boivin, N. Human Responses to Climate and Ecosystem Change in Ancient Arabia. Proc. Natl. Acad. Sci. USA 2020, 117, 8263–8270. [Google Scholar] [CrossRef] [Green Version]
  153. Kotwicki, V.; Al Sulaimani, Z. Climates of the Arabian Peninsula—Past, Present, Future. Int. J. Clim. Chang. Strateg. Manag. 2009, 1, 297–310. [Google Scholar] [CrossRef]
  154. Rustomji, N. The Garden and the Fire: Heaven and Hell in Islamic Culture; Columbia University Press: New York, NY, USA, 2008; 240p, ISBN 978-0-23151-183-4. [Google Scholar]
  155. Lange, C. Paradise and Hell in Islamic Traditions; Cambridge University Press: Cambridge, UK, 2016; ISBN 0-52-150637-9. [Google Scholar]
  156. Crown, A.D. Toward a Reconstruction of the Climate of Palestine 8000 B.C.–0 B.C. J. Near East. Stud. 1972, 31, 312–330. [Google Scholar] [CrossRef]
  157. Huntington, E. The Climate of Ancient Palestine. Part I. Bull. Am. Geogr. Soc. 1908, 40, 513–522. [Google Scholar] [CrossRef]
  158. Huntington, E. The Climate of Ancient Palestine. Part II. Bull. Am. Geogr. Soc. 1908, 40, 577–586. [Google Scholar] [CrossRef]
  159. Gregory, J.W. Palestine and the Stability of Climate in Historic Times. Geogr. J. 1930, 76, 487–494. [Google Scholar] [CrossRef]
  160. Ridderman, E. The Antinomy of Gehenna: Pavel Florensky’s Contribution to Debates on Hell and Universalism. Scott. J. Theol. 2021, 74, 235–251. [Google Scholar] [CrossRef]
  161. Bailey, L.R. Enigmatic Bible Passages: Gehenna: The Topography of Hell. Biblical Archaeol. 1986, 49, 187–191. [Google Scholar] [CrossRef]
  162. Shinn, G.W. What Has Become of Hell? North Am. Rev. 1900, 170, 837–849. [Google Scholar]
  163. Cohn-Sherbok, D. Judaism: History, Belief and Practice; Routledge: London, UK, 2003; ISBN 978-0-20340-251-1. [Google Scholar]
  164. Wright, J.E. The Early History of Heaven; Oxford University Press: Oxford, UK, 2002; ISBN 978-0-19515-230-2. [Google Scholar]
Figure 1. Pericles speech on Pnyx rock hill. Painting of Philipp Foltz. Wall painting in Maimileaneum Palace of Munich. From Wikimedia commons: https://commons.wikimedia.org/wiki/File:Discurso_funebre_pericles.PNG (accessed on 10 October 2022).
Figure 1. Pericles speech on Pnyx rock hill. Painting of Philipp Foltz. Wall painting in Maimileaneum Palace of Munich. From Wikimedia commons: https://commons.wikimedia.org/wiki/File:Discurso_funebre_pericles.PNG (accessed on 10 October 2022).
Atmosphere 13 01925 g001
Figure 2. The Elysium or Aeneas finding his father at the Elysian Fields, between 1597 and 1607, from the collection of the Museum of Fine Arts of Lyon in Lyon, France. It depicts a scene from Virgil’s Aeneid where Aeneas meets his father, Anchises in Elysium. From Wikimedia commons https://commons.wikimedia.org/wiki/File:Enee_meeting_with_his_father_in_the_Elysium-Sebastien_Vrancx-MBA_Lyon_H1153-IMG_0415.jpg (accessed on 10 October 2022).
Figure 2. The Elysium or Aeneas finding his father at the Elysian Fields, between 1597 and 1607, from the collection of the Museum of Fine Arts of Lyon in Lyon, France. It depicts a scene from Virgil’s Aeneid where Aeneas meets his father, Anchises in Elysium. From Wikimedia commons https://commons.wikimedia.org/wiki/File:Enee_meeting_with_his_father_in_the_Elysium-Sebastien_Vrancx-MBA_Lyon_H1153-IMG_0415.jpg (accessed on 10 October 2022).
Atmosphere 13 01925 g002
Figure 3. Sennedjem and Iineferti in the Fields of Iaru. From: https://www.metmuseum.org/art/collection/search/548354 (open access source) (accessed on 10 October 2022).
Figure 3. Sennedjem and Iineferti in the Fields of Iaru. From: https://www.metmuseum.org/art/collection/search/548354 (open access source) (accessed on 10 October 2022).
Atmosphere 13 01925 g003
Publisher’s Note: MDPI stays neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Share and Cite

MDPI and ACS Style

Charalampopoulos, I.; Matzarakis, A. Thoughts about the Thermal Environment and the Development of Human Civilisation. Atmosphere 2022, 13, 1925. https://doi.org/10.3390/atmos13111925

AMA Style

Charalampopoulos I, Matzarakis A. Thoughts about the Thermal Environment and the Development of Human Civilisation. Atmosphere. 2022; 13(11):1925. https://doi.org/10.3390/atmos13111925

Chicago/Turabian Style

Charalampopoulos, Ioannis, and Andreas Matzarakis. 2022. "Thoughts about the Thermal Environment and the Development of Human Civilisation" Atmosphere 13, no. 11: 1925. https://doi.org/10.3390/atmos13111925

APA Style

Charalampopoulos, I., & Matzarakis, A. (2022). Thoughts about the Thermal Environment and the Development of Human Civilisation. Atmosphere, 13(11), 1925. https://doi.org/10.3390/atmos13111925

Note that from the first issue of 2016, this journal uses article numbers instead of page numbers. See further details here.

Article Metrics

Back to TopTop